Prograding Dolerite Spires, Mount Wellington - Tasmania..Physical, chemical erosion and periglacial freeze and thaw cause boulders to move downslope. As the boulders move they lift up as they reach the edge a slope. Often this process causes mountain boulder streams.
Add to Cart Add to Lightbox Download- Filename
- anaspides-idw-0100-28-nov-2005.jpg
- Copyright
- © Iain D. Williams, All Rights Reserved. www.AnaspidesPhotography.net
- Image Size
- 4368x2912 / 6.4MB
- www.AnaspidesPhotography.net
- Contained in galleries
- LANDSCAPES & VISTAS
